全文获取类型
收费全文 | 9780篇 |
免费 | 2559篇 |
国内免费 | 3254篇 |
专业分类
测绘学 | 1758篇 |
大气科学 | 1362篇 |
地球物理 | 2010篇 |
地质学 | 6278篇 |
海洋学 | 1683篇 |
天文学 | 133篇 |
综合类 | 746篇 |
自然地理 | 1623篇 |
出版年
2024年 | 126篇 |
2023年 | 380篇 |
2022年 | 654篇 |
2021年 | 852篇 |
2020年 | 667篇 |
2019年 | 740篇 |
2018年 | 633篇 |
2017年 | 580篇 |
2016年 | 634篇 |
2015年 | 705篇 |
2014年 | 693篇 |
2013年 | 803篇 |
2012年 | 843篇 |
2011年 | 875篇 |
2010年 | 846篇 |
2009年 | 763篇 |
2008年 | 796篇 |
2007年 | 767篇 |
2006年 | 712篇 |
2005年 | 615篇 |
2004年 | 407篇 |
2003年 | 322篇 |
2002年 | 353篇 |
2001年 | 251篇 |
2000年 | 210篇 |
1999年 | 95篇 |
1998年 | 34篇 |
1997年 | 34篇 |
1996年 | 29篇 |
1995年 | 20篇 |
1994年 | 12篇 |
1993年 | 14篇 |
1992年 | 11篇 |
1991年 | 10篇 |
1990年 | 14篇 |
1989年 | 5篇 |
1988年 | 15篇 |
1987年 | 9篇 |
1986年 | 5篇 |
1985年 | 10篇 |
1983年 | 10篇 |
1982年 | 3篇 |
1981年 | 3篇 |
1979年 | 3篇 |
1978年 | 2篇 |
1965年 | 6篇 |
1964年 | 4篇 |
1963年 | 2篇 |
1962年 | 2篇 |
1954年 | 8篇 |
排序方式: 共有10000条查询结果,搜索用时 15 毫秒
11.
12.
13.
14.
During the Late Carboniferous to Early Permian, a rift was formed by post-collisional extension after ocean closure or an island arc-related basin formed by Paleo-Asian Ocean (PAO) subduction in the Xi Ujimqin area. Nevertheless, the closure time of the PAO is still under debate. Thus, to identify the origin of the PAO, the geochemistry and U-Pb age of zircons were analyzed for the extra-large deep marine, polymict clastic boulders and sandstones in the Shoushangou Formation within the basin. The analyses revealed magmatic activity and tectonic evolution. The conglomerates include megaclasts of granite (298.8 ± 9.1?Ma) and granodiorite porphyry (297.1 ± 3.1?Ma), which were deposited by muddy debris flow. Results of this study demonstrated that the boulders of granitoids have the geochemistry of typical I-type granite, characterized by low Zr + Nb + Ce + Y and low Ga/Al values. The granitoid boulders were formed in island arc setting, indicating the presence of arc magmatism in the area that is composed of the Late Carboniferous to Early Permian subduction-related granitoid in southern Xi Ujimqin. Multiple diagrams for determining sedimentary provenance using major and trace elements indicate that Shoushangou sediments originated from continental island arc-related felsic rocks. Detrital zircon U-Pb age cluster of 330–280?Ma was obtained, indicating input from granite, ophiolite, Xilin Gol complex, and Carboniferous sources to the south. The basin was geographically developed behind the arc during the Early Permian period because the outcropped intrusive rocks in the Late Carboniferous to Early Permian form a volcanic arc. The comprehensive analyses of source areas suggest that Shoushangou sediments developed in a backarc basin in response to the northward subduction of the PAO. The backarc basin and intrusive rocks, in addition to previously published Late Carboniferous to Early Permian magmatic rocks of arc unit in Xilin Gol, confirm the presence of an Early Permian trench-arc-basin system in the region, represented by the Baolidao arc and Xi Ujimqin backarc basin. This study highlights the importance and potential of combined geochemical and geochronological studies of conglomerates and sandstone for reconstructing the geodynamic setting of a basin. 相似文献
15.
16.
17.
皮肤图像分析系统对祛斑类化妆品功效评价的研究 总被引:13,自引:0,他引:13
目的是探索如何获得不同色素性皮肤病的清晰图像,研制出操作简单、自动化与精度高的皮肤图像分析系统。方法:应用多光谱皮肤显微偏振光与数字图像处理技术,测量目标皮损形状、面积、灰度、积分光密度及色素颜色参数的变化等。结果:用祛斑类化妆品和药物治疗136例黄褐斑、经该系统测量分析后各治疗组相关参数随时间的推移呈下降趋势,而药物组与对照组相比各参数值明显下降、与各组相比均有显著差异(P<0.05),并提出客观的疗效评定单位“ID”值。结论:该系统是一种潜力较大的皮肤表面色素定量工具,客观性和重复性好,灵敏度高,不对观察对象造成损伤,在临床获得满意效果。 相似文献
18.
马蔼乃 《地理与地理信息科学》2002,18(2):41-44
该文指出 :王化云的治黄思想 ,“上拦下排、两岸分滞、蓄水拦沙、宽河固堤、除害兴利、综合利用” ,实际上是治理黄河的系统工程 ,2 1世纪应该继承和发展黄河系统工程的方略。黄河地处中国腹地 ,是中华民族的摇篮 ,当今高新科技的发展 ,足以从更大的范围 ,以全国的水资源、土资源为核心来考虑黄河的建设。统一计算水资源中的大气水、地表水、地下水、壤中水、生态水、环境水、生产水、生活水 ;统一计算土资源中的土壤资源、沙资源、沙石资源 ,真正按照地理系统工程来建设黄河。 相似文献
19.
通过野外调查,在收集统计大量基础地质、经济地质、环境地质、旅游地质、农(林)业地质等数据信息的基础上,在GIS技术指导下,采用定量定性相结合的半定量分析评价方法,对森林浅覆盖区生态地质现状及各类资源的开发利用潜力进行了综合评价。在研究和探讨森林浅覆盖区生态地质综合评价方法的基础上,提出了森林浅覆盖区生态地质评价模型,确定了综合参数,划分了生态地质类型。 相似文献
20.
This paper designs three quasi-geostrophic barotropic models with a radial/horizontal grid length being 2 kin,one in the polar coordinates,one on a stationary typhoon circulation condition and another on a non-stationary typhoon circulation condition in the Cartesian coordinates,to investigate the effects of azimuthal and radial linear advections,and nonlinear advection on the inward propagation of mesoscale vorticity and the changes of typhoon intensity.Results show that the azimuthal linear advection may result in the formation of spiral vorticity bands;the radial linear advection in a certain parameter set is able to transfer vorticity inwards,leading to a slight enhancement of typhoon;the nonlinear advection of perturbation vorticity on a stationary typhoon circulation condition may transfer more vorticities inwards,thus resulting in a distinct enhancement of typhoon;and the nonlinear advection on a non-stationary typhoon circulation condition possesses duality,i.e.on the one hand,the advection increases the vorticity of inward propagation,thus favorable to the intensification of typhoon,and on the other hand,in the inward propagation process of vorticity the originally concentric and axisymmetric structure of typhoon basic flow is damaged,and a complex flow pattern forms,which in turn tends to weaken the circulation of typhoon.At last the paper discusses the possible applications of those results in typhoon intensity prediction. 相似文献